Mantle convection
= Mantle convection
{wiki}
Mantle convection is the slow buoyancy-driven motion of a rocky planetary mantle. On geological timescales the solid mantle behaves as a highly viscous <Newtonian fluid> to first approximation.
= Mantle convection
{wiki}
Mantle convection is the slow buoyancy-driven motion of a rocky planetary mantle. On geological timescales the solid mantle behaves as a highly viscous <Newtonian fluid> to first approximation.